Fig. 5.From: Deep structure of the Ou mountain range strain concentration zone and the focal area of the 2008 Iwate-Miyagi Nairiku earthquake, NE Japan—seismogenesis related with magma and crustal fluidResult of the checkerboard resolution test. We used the synthetic checkerboard pattern on a scale of about 10 km. Others are the same as Fig. 4.Back to article page